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    This section needs additional citations for verification. Please help improve this article by adding citations to reliable sources. Unsourced material may be challenged and removed. Outcrops of granite tend to form tors and rounded massifs. Granites sometimes occur in circular depressions surrounded by a range of hills, formed by the metamorphic aureole or hornfels.

    Small dikes of granitic composition called aplites are often associated with the margins of granitic intrusions. In some locations, very coarse-grained pegmatite masses occur with granite. Origin[ edit ] Granite has a felsic composition and is more common in recent geologic time in contrast to Earth's ultramafic ancient igneous history. Felsic rocks are less dense than mafic and ultramafic rocks, and thus they tend to escape subductionwhereas basaltic or gabbroic rocks tend to sink into the mantle beneath the granitic rocks of the continental cratons.

    Therefore, granitic rocks form the basement of all land continents. Geochemical origins[ edit ] Granitoids have crystallized from magmas that have compositions at or near a eutectic point or a temperature minimum on a cotectic curve. Magmas will evolve to the eutectic because of igneous differentiationor because they represent low degrees of partial melting. Fractional crystallisation serves to reduce a melt in ironmagnesiumtitaniumcalcium and sodiumand enrich the melt in potassium and silicon — alkali feldspar rich in potassium and quartz SiO2are two of the defining constituents of granite.

    This process operates regardless of the origin of the parental magma to the granite, and regardless of its chemistry. However, the composition and origin of the magma that differentiates into granite leaves certain geochemical and mineral evidence as to what the granite's parental rock was. The final mineralogy, texture and chemical composition of a granite is often distinctive as to its origin.

    For instance, a granite that is formed from melted sediments may have more alkali feldsparwhereas a granite derived from melted basalt may be richer in plagioclase feldspar. It is on this basis that the modern "alphabet" classification schemes are based. Granite has a slow cooling process which forms larger crystals. M-type or mantle derived granite was later proposed to cover those granites that were clearly sourced from crystallized mafic magmas, generally sourced from the mantle.

    These are rare, because it is difficult to turn basalt into granite via fractional crystallisation. A-type or anorogenic granites are formed above volcanic "hot spot" activity and have a peculiar mineralogy and geochemistry.

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    These granites are formed by the melting of the lower crust under conditions that are usually extremely dry. The rhyolites of the Yellowstone Caldera are examples of volcanic equivalents of A-type granite. Granitization[ edit ] An old, and largely discounted theory, granitization states that granite is formed in place by extreme metasomatism by fluids bringing in elements, e.

    This was supposed to occur across a migrating front. The production of granite by metamorphic heat is difficult, but is observed to occur in certain amphibolite and granulite terrains.

    In-situ granitisation or melting by metamorphism is difficult to recognise except where leucosome and melanosome textures are present in migmatites. Once a metamorphic rock is melted it is no longer a metamorphic rock and is a magma, so these rocks are seen as a transitional between the two, but are not technically granite as they do not actually intrude into other rocks.

    In all cases, melting of solid rock requires high temperature, and also water or other volatiles which act as a catalyst by lowering the solidus temperature of the rock. Ascent and emplacement[ edit ] The ascent and emplacement of large volumes of granite within the upper continental crust is a source of much debate amongst geologists.

    There is a lack of field evidence for any proposed mechanisms, so hypotheses are predominantly based upon experimental data. There are two major hypotheses for the ascent of magma through the crust: Fracture propagation Of these two mechanisms, Stokes diapir was favoured for many years in the absence of a reasonable alternative.

    The basic idea is that magma will rise through the crust as a single mass through buoyancy. As it rises, it heats the wall rockscausing them to behave as a power-law fluid and thus flow around the pluton allowing it to pass rapidly and without major heat loss.

    Rocks there do not deform so easily: Fracture propagation is the mechanism preferred by many geologists as it largely eliminates the major problems of moving a huge mass of magma through cold brittle crust. Magma rises instead in small channels along self-propagating dykes which form along new or pre-existing fracture or fault systems and networks of active shear zones.

    Granitic magma must make room for itself or be intruded into other rocks in order to form an intrusion, and several mechanisms have been proposed to explain how large batholiths have been emplaced: Stopingwhere the granite cracks the wall rocks and pushes upwards as it removes blocks of the overlying crust Assimilation, where the granite melts its way up into the crust and removes overlying material in this way Inflation, where the granite body inflates under pressure and is injected into position Most geologists today accept that a combination of these phenomena can be used to explain granite intrusions, and that not all granites can be explained entirely by one or another mechanism.

    Weathering Grus sand and granitoid it derived from Physical weathering occurs on a large scale in the form of exfoliation jointswhich are the result of granite's expanding and fracturing as pressure is relieved when overlying material is removed by erosion or other processes. Chemical weathering of granite occurs when dilute carbonic acidand other acids present in rain and soil waters, alter feldspar in a process called hydrolysis.

    An end product of granite weathering is gruswhich is often made up of coarse-grained fragments of disintegrated granite. For about two thousand years, the relief engravings on Cleopatra's Needle obelisk had survived the arid conditions of its origin before its transfer to London. Within two hundred years, the red granite has drastically deteriorated in the damp and polluted air there.

    Potassium is a radioactive isotope of weak emission, and a constituent of alkali feldsparwhich in turn is a common component of granitic rocks, more abundant in alkali feldspar granite and syenites. Naturally, a geiger counter should register this low effect. Some granites contain around 10 to 20 parts per million ppm of uranium. By contrast, more mafic rocks, such as tonalite, gabbro and dioritehave 1 to 5 ppm uranium, and limestones and sedimentary rocks usually have equally low amounts.

    Many large granite plutons are sources for palaeochannel -hosted or roll front uranium ore depositswhere the uranium washes into the sediments from the granite uplands and associated, often highly radioactive pegmatites. Cellars and basements built into soils over granite can become a trap for radon gas, which is formed by the decay of uranium. Dan Steck of St. Various resources from national geological survey organizations are accessible online to assist in assessing the risk factors in granite country and design rules relating, in particular, to preventing accumulation of radon gas in enclosed basements and dwellings.

    A study of granite countertops was done initiated and paid for by the Marble Institute of America in November by National Health and Engineering Inc. In this test, all of the 39 full-size granite slabs that were measured for the study showed radiation levels well below the European Union safety standards section 4.

    Granite and related marble industries are considered one of the oldest industries in the world; existing as far back as Ancient Egypt. Menkaure's Pyramidlikely dating to the same era, was constructed of limestone and granite blocks. The Great Pyramid of Giza c. The mostly ruined Black Pyramid dating from the reign of Amenemhat III once had a polished granite pyramidion or capstone, which is now on display in the main hall of the Egyptian Museum in Cairo see Dahshur.

    Other uses in Ancient Egypt include columnsdoor lintelssillsjambsand wall and floor veneer. Patrick Hunt [27] has postulated that the Egyptians used emerywhich has greater hardness on the Mohs scale.

    The Brihadeeswarar Temple dedicated to Lord Shiva was built in The massive Gopuram ornate, upper section of shrine is believed to have a mass of around 81 tonnes. It was the tallest temple in south India.

    Granite became "an integral part of the Roman language of monumental architecture". Beginning in Late Antiquity the granite was reused, which since at least the early 16th century became known as spoliation. Through the process of case-hardeninggranite becomes harder with age.

    The technology required to make tempered steel chisels was largely forgotten during the Middle Ages. As a result, Medieval stoneworkers were forced to use saws or emery to shorten ancient columns or hack them into discs. Giorgio Vasari noted in the 16th century that granite in quarries was "far softer and easier to work than after it has lain exposed" while ancient columns, because of their "hardness and solidity have nothing to fear from fire or sword, and time itself, that drives everything to ruin, not only has not destroyed them but has not even altered their colour.

    Granite is a hard stone and requires skill to carve by hand. Until the early 18th century, in the Western world, granite could be carved only by hand tools with generally poor results. A key breakthrough was the invention of steam-powered cutting and dressing tools by Alexander MacDonald of Aberdeeninspired by seeing ancient Egyptian granite carvings. Inthe first polished tombstone of Aberdeen granite to be erected in an English cemetery was installed at Kensal Green Cemetery.

    It caused a sensation in the London monumental trade and for some years all polished granite ordered came from MacDonald's. The royal sarcophagus at Frogmore was probably the pinnacle of its work, and at 30 tons one of the largest. It was not until the s that rival machinery and works could compete with the MacDonald works. Modern methods of carving include using computer-controlled rotary bits and sandblasting over a rubber stencil. Leaving the letters, numbers, and emblems exposed on the stone, the blaster can create virtually any kind of artwork or epitaph.

    The stone known as "black granite" is usually gabbrowhich has a completely different chemical composition. Aberdeen in Scotland, which is constructed principally from local granite, is known as "The Granite City".

    Because of its abundance in New Englandgranite was commonly used to build foundations for homes there. The Granite RailwayAmerica's first railroad, was built to haul granite from the quarries in Quincy, Massachusettsto the Neponset River in the s. Engineering[ edit ] Engineers have traditionally used polished granite surface plates to establish a plane of reference, since they are relatively impervious and inflexible.

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    Sandblasted concrete with a heavy aggregate content has an appearance similar to rough granite, and is often used as a substitute when use of real granite is impractical. A most unusual use of granite was as the material of the tracks of the Haytor Granite TramwayDevon, England, in Granite block is usually processed into slabs, which can be cut and shaped by a cutting center. Granite tables are used extensively as bases for optical instruments because of granite's rigidity, high dimensional stability, and excellent vibration characteristics.

    In military engineering, Finland planted granite boulders along its Mannerheim Line to block invasion by Russian tanks in the winter war of Other uses[ edit ] Curling stones are traditionally fashioned of Ailsa Craig granite. The first stones were made in the s, the original source being Ailsa Craig in Scotland.

    Between 60 and 70 percent of the stones used today are made from Ailsa Craig granite, although the island is now a wildlife reserve and is still used for quarrying under license for Ailsa granite by Kays of Mauchline for curling stones. Granite rock climbing is so popular that many of the artificial rock climbing walls found in gyms and theme parks are made to look and feel like granite.

    Granite was used for setts on the St.
    These Croatian glagolitic Lenten chants retrace a venerable and direct link to our ancestors, our roots, and our religious belief.

    Born out of Middle Ages, they continue to extend an unbroken tradition of Croatian history.

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    They still resonate as part of our being, so let them be our pride, our support, and our hope. Gospin plac - Madonna's weeping Stabat mater dolorosa [ mp3 ]. Tebe Boga hvalimo Te Deum [ wma ] See Pasionska bastina page in Croatianand listen to Madonna's weeping Stabat mater dolorosaa glagolitic chant from the island of Hvar village of Vrbanja. Truly amazing way of singing be patient while listening. Leos Janacek, Czechia, composed his famous Glagolitic Mass.

    The oldest known music preserved in Croatian language is considered to be Kantual "Blagoslovimo Gospodina" Let us Bless Lordwritten in Latin Script, dating from the end of 14th till the beginning of 16th centuries. It is kept in the Dominican Convent in Starigrad on the island of Hvar. Croatian Middle Age Musicby Hana Breko in Croatian Glagolitic singingby Gorana Doliner in Croatian Petar Hektorovic, a well known Croatian poet, nobleman, connoisseur of Latin language and classical literature, wrote his Ribanje i ribarsko prigovaranje inwhich is the first realistic epic poem of Croatian Renaissance literature.

    It provides four folk tunes accompanied with musical notation. The book has been translated from Croatian into English in by Edward Dennis Goy under the title Fishing and fisherman's' conversation. Bartol Gyurgieuvitsborn in Turopolje near Zagreb, had spent 14 years enslaved in Turkish Empire.

    After his escape to Europe he published numerous works about the Turks. Among them is De Turcarum ritu et caeremoniis where he is called Bartholomeus Georgievitspublished in Amsterdam inin which he described among others the characteristics of music in Islamic society. It was among the first in Europe treating Islamic music, and was translated into seven languages.

    It was indeed very popular throughout Europe: Juraj Husa Croatian captive in Turkey, became a military trumpeter for the Turkish army. Once he played his trumpet on the top of a pyramid near Cairo, 16th century! The Croats can boast of having two excellent Renaissance composers. The first one is Julije Skjavetic Schiavetti from the 16th century. Between and he lived in Sibenik, and was conducting a choir in the famous Sibenik Cathedral.

    He wrote a collection of madrigals for voices and a collection of motets for voices both published in Venice in and respectively. An important collection of his motets that was held in Dresden, disappeared after the destruction of the city in Luckily, it was discovered in Krakow in According to [ Miho DemovicAndjelko Klobucar, p. The earliest known documents testifying to existence of organs in Croatia are from Zagreb and Dubrovnik Ivan Lukacica Renaissance composer born in Sibenik, was conductor and organist in the Split Cathedral.

    In he published a collection Sacrae cantiones, containing 27 motets for voices accompanied by organs. Lukacic's collection was lost in the course of WW2, and rediscovered in the 's at the Jagiellon Library in Krakow, Poland.

    This is the only known copy. Gabriello Pulitian Italian priest, was an important composer for lute and organ in various Croatian towns of Istria. Another interesting Italian composer was Tomaso Cechinian organist in the cathedral in Split and Hvar on the island of Hvar. Both of them influenced the Croatian cultural circle in this region. Besides Lukacic, Vinko Jelic was the most important representative of Croatian church music of the time.

    He was born in Rijeka, and died in Alsace in France Zabern. This Early Baroque composer is noted for introducing new techniques like chromatics and sequences into his music, which have just begun to appear in Europe. In he published a collection consisting of 24 motets plus 4 other pieces Parnassia militia in Strassbourg. It is important in its language, text and sheet music.

    Paulists left important traces in Croatian culture during five centuries of their presence in Croatian lands from 13th to 18th centuries, see [ Sekulic ]. It was published in Vienna in Many thanks to dr. According to outstanding Croatian ecumenist, theologist and musicologist Juraj Krizanicmusic should be regarded as a part of mathematics. In Rome he supervised a publication of musical works of the Portuguese king D.

    It was the first history of Venetian opera, covering the period of - Its 2nd edition appeared in In various cities in northern Italy and in smaller number in Dalmatian part of Croatia Nerezisce and Supetar on the island of Brac, the Cathedral of Rab on the island of Rab, church of St.

    Frane in Sibenik, Visovac covent on the Krka river his workshop built more than top quality organs according to some data - more than ! He built sophisticated organs for the grand basilica in Padova with 30 registers and 2 manualsbut it disappeared in the fire in He also introduced some innovations in the construction of organs tiratutti that are in use even today, found new tonal ratios mensura'sand founded a unique school for organ building in Venice.

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    Cithara Octochorda is the most significant old collection of Latin - Croatian Church songs, published in in Vienna, reprinted in again in Vienna, and in in Zagreb. This impressive, monumental book contains Croatian songs in the Kajkavian dialect. The songs were a part of the so called Old Zagreb Rite the official Croatian name was Stari Zagrebacki obred, founded in the course of 11th and 12th centuriesthat was cancelled in and replaced by Roman Rite.

    According to [ Korner and Demovic ] the edition of Cithara Octochorda was the first printed book in Croatia containing sheet music of Croatian songs. Cithara Octhocorda each of its pp can be viewed at the National and University Library in Zagreb. The Old Zagreb Rite mentioned above had been used in the Zagreb Bishopric, which at that time was much larger than today.

    It was probably also used in Istria and in the Senj Bishopric. The cancellation of the Old Zagreb Rite in after approximately seven centuries of existence certainly included the Zagreb Cathedral, but numerous churches still continued to use the Rite.

    The first printed Missal and the only one according to the Old Zagreb Rite had been published already in Personal information by dr. Miho Demovic in See also the articles by [ Hana Breko ] and [ Josip degl'Ivellio ]. He later spent some considerable time teaching in the town of Trnava in modern Slovakia.

    Luka Sorkocevicwhose beautiful symphonies are performed throughout the world, lived in Dubrovnik. The opening melody to this web page is his Allegro. Sorkocevic was born 22 years before Mozart. You can see a detail from the Dubrovnik polyptich by Lovro Dobricevic fromrepresenting an angel playing portative, a small portable organ: Ivan Mane Jarnovic Italianized name Giornovichi, was an outstanding Croatian violinist and composer of the 18th century, probably from Dubrovnik.

    Also played the first violin in the orchestra of the Russian empress Katarina II. Jarnovic composed about 50 chamber instrumental pieces, 22 violin concerts 17 preservedand is known for having introduced the romanza as a slow movement into the structure of the violin concert.

    Many inspired fans of Jarnovic's beautiful concerts enlisted in lessons for beginners in the hopes of one day being able to emulate the man. His life is described in a novel Jarnowick by G. The earliest known symphonic orchestra in Croatia has been founded in Dubrovnik It is a testimony of the Croatian musical Gregorian-plainsong tradition.

    It consists of six dialogues discussing the emergence of music and singing staff, notes and keys.

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